刘冬雁, 彭莎莎, 乔彦松, 谢瑞煌. 青藏高原东南缘甘孜黄土磁化率揭示的西南季风演化[J]. 海洋地质与第四纪地质, 2009, 29(5): 115-121. DOI: 10.3724/SP.J.1140.2009.05115
引用本文: 刘冬雁, 彭莎莎, 乔彦松, 谢瑞煌. 青藏高原东南缘甘孜黄土磁化率揭示的西南季风演化[J]. 海洋地质与第四纪地质, 2009, 29(5): 115-121. DOI: 10.3724/SP.J.1140.2009.05115
LIU Dongyan, PENG Shasha, QIAO Yansong, XIE Ruihuang. EVOLUTION OF THE SOUTHWEST MONSOON ON ORBITAL TIME-SCALE REVEALED BY A LOESS-PALEOSOL SEQUENCE ON THE SOUTHEASTERN MARGIN OF THE QINGHAI-TIBETAN PLATEAU FOR THE LAST 1.16 Ma[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 115-121. DOI: 10.3724/SP.J.1140.2009.05115
Citation: LIU Dongyan, PENG Shasha, QIAO Yansong, XIE Ruihuang. EVOLUTION OF THE SOUTHWEST MONSOON ON ORBITAL TIME-SCALE REVEALED BY A LOESS-PALEOSOL SEQUENCE ON THE SOUTHEASTERN MARGIN OF THE QINGHAI-TIBETAN PLATEAU FOR THE LAST 1.16 Ma[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 115-121. DOI: 10.3724/SP.J.1140.2009.05115

青藏高原东南缘甘孜黄土磁化率揭示的西南季风演化

EVOLUTION OF THE SOUTHWEST MONSOON ON ORBITAL TIME-SCALE REVEALED BY A LOESS-PALEOSOL SEQUENCE ON THE SOUTHEASTERN MARGIN OF THE QINGHAI-TIBETAN PLATEAU FOR THE LAST 1.16 Ma

  • 摘要: 以青藏高原东南缘甘孜A剖面黄土-古土壤序列为材料,在磁性地层学研究的基础上,对其高分辨率磁化率记录的多时间尺度气候特征进行了分析。磁性地层学研究结果表明,甘孜A剖面典型风尘堆积的底界年龄约为1.16 Ma。磁化率记录在构造时间尺度上具有明显的阶段性,显示了西南季风演化存在中更新世气候转型。功率谱分析检出典型的偏心率100 ka、斜率41 ka、岁差23 ka轨道周期和11.4、7.5 ka的岁差拍頻周期,指示西南季风演化受天文因素影响,印度季风系统对太阳辐射具有非线性响应和热带特征。

     

    Abstract: Climatic characteristics of different stages recorded by high-resolution magnetic susceptibility are discussed based on loess-paleosol sequence of Garzê A section and also on magnetostratigraphy on the southeastern margin of the Qinghai-Tibetan Plateau.Periodicities of the earth's orbital parameters are detected by power spectral analysis and the evolution of the southwest monsoon on orbital time-scale is studied.The results show that (1) the cycle of quasi-100 ka does exsit in the evolution of the southwest monsoon, and the obliquity cycle and precession cycle are remarkably detected as well;(2) the beat frequency periods of the precession are detected and give a strong non-linear response to the solar insolation and the tropical climatic characteristics of the southwest monsoon;(3) the mid-Pleistocene transition which was recognized in the evolution of the southwest monsoon began approximately 0.95 MaBP and ended around 0.6 MaBP.

     

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